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  2. Laccolith - Wikipedia

    en.wikipedia.org/wiki/Laccolith

    A laccolith is a type of igneous intrusion, formed when magma forces its way upwards through the Earth's crust but cools and solidifies before reaching the surface. Laccoliths are distinguished from other igneous intrusions by their dome-shaped upper surface and level base. They are assumed to be fed by a conduit from below, though this is ...

  3. Mount Bachelor - Wikipedia

    en.wikipedia.org/wiki/Mount_Bachelor

    Ski lifts. Mount Bachelor, formerly named Bachelor Butte, is a dormant stratovolcano atop a shield volcano in the Cascade Volcanic Arc and the Cascade Range of central Oregon, United States. Named Mount Bachelor because it stands apart from the nearby Three Sisters, [4] it lies in the eastern segment of the central portion of the High Cascades ...

  4. Submarine volcano - Wikipedia

    en.wikipedia.org/wiki/Submarine_volcano

    Submarine volcanoes are underwater vents or fissures in the Earth 's surface from which magma can erupt. Many submarine volcanoes are located near areas of tectonic plate formation, known as mid-ocean ridges. The volcanoes at mid-ocean ridges alone are estimated to account for 75% of the magma output on Earth. [1]

  5. 1902 eruption of Mount Pelée - Wikipedia

    en.wikipedia.org/wiki/1902_eruption_of_Mount_Pelée

    The tsunamis swept along the coast, damaging buildings and boats. The explosions resumed the night of 5 May. The following morning, parts of the eruption plume became incandescent, signifying that the character of the eruption had changed. The phreatic eruptions had finally given way to magmatic eruptions as magma reached the surface. These ...

  6. Campanian Ignimbrite eruption - Wikipedia

    en.wikipedia.org/wiki/Campanian_Ignimbrite_eruption

    The structure's magma chamber remains active as there apparently are solfataras, hot springs, gas emissions and frequent episodes of large-scale up- and downlift ground deformation do occur. [18] [19] In 2008 it was discovered that the Phlegraean Fields and Mount Vesuvius have a common magma chamber at a depth of 10 km (6.2 mi). [20]

  7. Geology of the Lassen volcanic area - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Lassen...

    2; the higher the silica content, the greater the ability of the magma to trap and hold on to gas and water vapor. When high-silica magma rises to the Earth's surface, the trapped gases and vapors can erupt explosively to produce ash clouds and pyroclastic flows that consist of superheated gas, ash and volcanic fragments.

  8. Mount Mazama - Wikipedia

    en.wikipedia.org/wiki/Mount_Mazama

    Mount Scott, at a height of 8,934 feet (2,723 m), [34] marks the oldest visible remnant of this original cluster. [35] Scott was the first of the composite volcanoes that created the Mazama complex, formed by a quick and active cone-building phase and becoming inactive long before the most recent eruption at Mazama.

  9. Bermuda rig - Wikipedia

    en.wikipedia.org/wiki/Bermuda_rig

    1671 woodcut of a Bermudian vessel with early Bermuda rig (before the addition of a boom). The rig consists of a triangular sail set aft of the mast with its mainsail raised to the top of the mast; its luff runs down the mast and is normally attached to it for its entire length; its tack is attached at the base of the mast; its foot (in modern versions of the rig) controlled by a boom; and its ...

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